Hydrological Characteristics and Key Influencing Factors of Typical Lakes in the Qinghai Tibet Plateau from 1985 to 2021

ZHANG Jiaqi; ZHANG Huilan; LIU Xueyan

doi:10.13870/j.cnki.stbcxb.2024.03.025

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Hydrological Characteristics and Key Influencing Factors of Typical Lakes in the Qinghai Tibet Plateau from 1985 to 2021

更新时间：2025-03-12

- Hydrological Characteristics and Key Influencing Factors of Typical Lakes in the Qinghai Tibet Plateau from 1985 to 2021
- Vol. 38, Issue 3, Pages: 140-149(2024)
- 作者机构：
  
  1. 北京林业大学水土保持学院,北京,100083
  2. 北京林业大学重庆缙云三峡库区森林生态系统国家定位观测研究站,重庆,400711
- 作者简介：
- 基金信息：
- DOI：10.13870/j.cnki.stbcxb.2024.03.025
  CLC： P333.6
- Published：2024
- 稿件说明：
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ZHANG Jiaqi, ZHANG Huilan, LIU Xueyan. Hydrological Characteristics and Key Influencing Factors of Typical Lakes in the Qinghai Tibet Plateau from 1985 to 2021[J]. 2024, 38(3): 140-149.
DOI：

ZHANG Jiaqi, ZHANG Huilan, LIU Xueyan. Hydrological Characteristics and Key Influencing Factors of Typical Lakes in the Qinghai Tibet Plateau from 1985 to 2021[J]. 2024, 38(3): 140-149. DOI： 10.13870/j.cnki.stbcxb.2024.03.025.

摘要

[目的] 青藏高原的湖泊是气候变化的重要指示器

其扩张或缩减亦对青藏高原自然环境产生重要影响。[方法] 选取位于青藏高原不同气候子区的3个典型湖泊(青海湖、羊卓雍错、乌兰乌拉湖)

采用遥感监测手段

研究3个典型湖泊1985—2021年水文特征的时空变化规律

揭示关键气候因子的作用

并进一步探讨冰川和冻土对典型湖泊的影响。[结果] 研究期间

青海湖的面积和水位呈显著上升趋势

面积增长238.68 km2

水位增长1.32 m

空间上则向东西方向扩张;羊卓雍错湖泊面积呈先波动上升后减少趋势

面积和水位分别减少16.31 km2和3.25 m

在空间上整体由四周向中心的萎缩态势;乌兰乌拉湖面积和水位呈显著上升趋势

分别增长125.57 km2和8.12 m

扩张区域主要集中在南部。[结论] 在暖湿化环境下

降水增多和冰川冻土加速融化导致的湖泊扩张是青藏高原最为突出的环境变化特征

其中

降水量变化是影响青海湖和羊湖面积变化的关键因素

且面积变化和降水量具有滞后性;而乌兰乌拉湖水位上升的主要原因是气温升高引起冻土的季节融化。探索青藏高原湖泊面积的变化

对深入研究全球气候变化及地表水资源评估具有重要指导意义。

Abstract

[Objective] The lakes of the Tibetan Plateau are important indicators of climate change

and their expansion or contraction also have an important impact on the natural environment of the Tibetan Plateau. [Methods] Three typical lakes located in different climatic sub-regions of the Qinghai-Tibet Plateau (Qinghai Lake

Yangzhuo Yongcuo

and Ulan Ula Lake) were selected to study the temporal and spatial variation of the hydrological characteristics of the three typical lakes from 1985 to 2021 by remote sensing monitoring methods

to reveal the role of key climatic factors

and to further explore the influence of glaciers and permafrost on the typical lakes. [Results] The area and water level of Qinghai Lake showed a significant upward trend

with an area increase of 238.68 km2 and a water level increase of 1.32 m. In space

it showed a trend of expansion in the east-west direction. The area and water level of Yangzhuo Yongcuo Lake first fluctuated and then decreased

decreasing by 16.31 km2 and 3.25 m respectively. In space

the overall area showed a shrinking trend from the surrounding to the center. The area and water level of Ulan Ula Lake showed a significant upward trend

increasing by 125.57 km2 and 8.12 m

respectively

and the expansion area was mainly concentrated in the south. [Conclusion] The analysis of key climate factors shows that the lake expansion caused by the increase of precipitation and the accelerated melting of glacial permafrost in the warm and humid environment is the most prominent environmental change characteristics of the Qinghai-Tibet Plateau. The main reason for the rise in the water level of Ulan Ula Lake is the seasonal thaw of permafrost caused by rising temperatures. Exploring the changes in lake area on the Tibetan Plateau is of great guiding significance for in-depth research on global climate change and surface water resource assessment.

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references

詹鹏飞,刘凯,张玉超,等.青藏高原不同气候子区典型湖泊多时间尺度变化的遥感对比研究[J].遥感技术与应用,2021,36(1):90-102. ZHAN P F, LIU K, ZHANG Y C, et al. A comparative study on the changes of typical lakes in different climate zones of the Tibetan Plateau at multi-timescales based on remote sensing observations[J].Remote Sensing Technology and Application,2021,36(1):90-102.

袁烽迪,张溪,魏永强.青藏高原生态屏障区生态环境脆弱性评价研究[J].地理空间信息,2018,16(4):67-69,10. YUAN F D, ZHANG X, WEI Y Q. Evaluation of ecological environment vulnerability in the Qinghai-Tibet Plateau ecological barrier zone[J].Geospatial Information,2018,16(4):67-69,10.

SU Z, SHI Y F, ZHENG B X. Quaternary glacier monuments and ice age division of Gongga Mountain[J].Advances in Earth Science,2002(5):639-647.

姚檀栋,朱立平.青藏高原环境变化对全球变化的响应及其适应对策[J].地球科学进展,2006,21(5):459-464. YAO T D, ZHU L P. Theresponse of environmental changes on Tibetan Plateau to global changes and adaptation strategy[J].Advances in Earth Science,2006,21(5):459-464.

ZHANG G Q, LUO W, CHEN W F, et al. A robust but variable lake expansion on the Tibetan Plateau[J].Science Bulletin,2019,64(18):1306-1309.

陈军,刘延昭,曹立国,等.青藏高原湖泊变化遥感监测及水量平衡定量估算研究进展[J].冰川冻土,2022,44(4):1203-1215. CHEN J, LIU Y Z, CAO L G, et al. A review on the research of remote sensing monitoring of lake changes and quantitative estimation of lake water balance in Qinghai-Tibet Plateau[J].Journal of Glaciology and Geocryology,2022,44(4):1203-1215.

张国庆.青藏高原湖泊变化遥感监测及其对气候变化的响应研究进展[J].地理科学进展,2018,37(2):214-223. ZHANG G Q. Changes in lakes on the Tibetan Plateau observed from satellite data and their responses to climate variations[J].Progress in Geography,2018,37(2):214-223.

孟庆伟.青藏高原特大型湖泊遥感分析及其环境意义[D].北京:中国地质科学院,2007. MENG Q W. Remote sensing analysis of the large lakes in the Tibetan Plateau and its environmental significance[D]. Beijing:Chinese Academy of Geological Sciences,2007.

武慧智,姜琦刚,程彬.基于RS和GIS技术青藏高原湖泊动态变化研究[J].世界地质,2007,26(1):66-70. WU H Z, JIANG Q G, CHENG B. Study of dynamic changes of lakes in Qinghai-Tibet Plateau based on remote sensing and GIS[J].Global Geology,2007,26(1):66-70.

董斯扬,薛娴,尤全刚,等.近40年青藏高原湖泊面积变化遥感分析[J].湖泊科学,2014,26(4):535-544. DONG S Y, XUE X, YOU Q G, et al. Remote sensing monitoring of the lake area changes in the Qinghai-Tibet Plateau in recent 40 years[J].Journal of Lake Sciences,2014,26(4):535-544.

王文种,黄对,刘九夫,等.基于Landsat与Sentinel-3A卫星数据的当惹雍错1988—2018年湖泊水位—水量变化及归因[J].湖泊科学,2020,32(5):1552-1563. WANG W Z, HUANG D, LIU J F, et al. Patterns and causes of changes in water level and volume in Tangra Yumco from 1988 to 2018 based on Landsat images and Sentinel-3A synthetic aperture radar[J].Journal of Lake Sciences,2020,32(5):1552-1563.

郭丰杰,李婷,季民.2000—2019年青海湖面积时序特征分析及预测[J].科学技术与工程,2022,22(2):740-748. GUO F J, LI T, JI M, et al. Time series analysis and prediction of Qinghai Lake area from 2000 to 2019[J]. Science Technology and Engineering,2022,22(2):740-748.

闾利,张廷斌,易桂花,等.2000年以来青藏高原湖泊面积变化与气候要素的响应关系[J].湖泊科学,2019,31(2):573-589. LÜ L, ZHANG T B, YI G H, et al. Changes of lake areas and its response to the climatic factors in Tibetan Plateau since 2000[J].Journal of Lake Sciences,2019,31(2):573-589.

朱立平,鞠建廷,乔宝晋,等."亚洲水塔"的近期湖泊变化及气候响应:进展、问题与展望[J].科学通报,2019,64(27):2796-2806. ZHU L P, JU J T, QIAO B J, et al. Recent lake changes of the Asia Water Tower and their climate response: Progress, problems and prospects[J].Chinese Science Bulletin,2019,64(27):2796-2806.

朱立平,谢曼平,吴艳红.西藏纳木错1971-2004年湖泊面积变化及其原因的定量分析[J].科学通报,2010,55(18):1789-1798. ZHU L P, XIE M P, WU Y H. Quantitative analysis of lake area change and its causes in Namco, Tibet from 1971 to 2004[J].Chinese Science Bulletin,2010,55(18):1789-1798.

李晟铭,刘吉平,刘阁,等.三个时期青藏高原冰川补给型湖泊的变化[J].湿地科学,2018,16(2):130-137. LI S M, LIU J P, LIU G, et al. Changes of glacier-fed lakes in Tibetan Plateau for three periods[J].Wetland Science,2018,16(2):130-137.

朱立平,彭萍,张国庆,等.全球变化下青藏高原湖泊在地表水循环中的作用[J].湖泊科学,2020,32(3):597-608. ZHU L P, PENG P, ZHANG G Q,et al. The role of Tibetan Plateau Lakes in surface water cycle under global changes[J].Journal of Lake Sciences,2020,32(3):597-608.

张洪源,吴艳红,刘衍君,等.近20年青海湖水量变化遥感分析[J].地理科学进展,2018, 37(6): 823-832. ZHANG H Y, WU Y H, LIU E, et al. Water storage variation of the Qinghai Lake in recent decades based on satellite observation[J]. Progress in Geography, 2018, 37(6): 823-832.

谭春萍,杨建平,米睿.1971—2007年青藏高原南部气候变化特征分析[J].冰川冻土,2010,32(6):1111-1120. TAN C P, YANG J P, MI R. Analysis of the climatic change characteristics in the southern Tibetan Plateau from 1971 to 2007[J].Journal of Glaciology and Geocryology,2010,32(6):1111-1120.

赵永利.西藏羊卓雍错流域冰川-湖泊动态变化研究[J].干旱区资源与环境,2014,28(8):88-93. ZHAO Y L. Dynamic variations of glaciers-lake in YamzhoYumco Basin of Tibet[J].Journal of Arid Land Resources and Environment,2014,28(8):88-93.

除多,普穷,拉巴卓玛,等.近40 a西藏羊卓雍错湖泊面积变化遥感分析[J].湖泊科学,2012,24(3):494-502. CHU D,PU Q, L B Z M, et al. Remote sensing analysis on lake area variations of Yamzho Yumco in Tibetan Plateau over the past 40 a[J]. Lake Science,2012,24(3):494-502.

李韧,赵林,丁永建,等.青藏公路沿线多年冻土区活动层动态变化及区域差异特征[J].科学通报,2012,57(30):2864-2871. LI R, ZHAO L, DING Y J, et al. Dynamic change and regional difference characteristics of active layer in permafrost region along Qinghai-Tibet highway[J].Chinese Science Bulletin,2012,57(30):2864-2871.

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